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关于使用过剩熵缩放来描述水的动态特性。

On the use of excess entropy scaling to describe the dynamic properties of water.

机构信息

Department of Chemical and Biological Engineering, University at Buffalo, The State University of New York, Buffalo, New York 14260, USA.

出版信息

J Phys Chem B. 2010 Aug 19;114(32):10558-66. doi: 10.1021/jp1049155.

Abstract

We use molecular dynamics and transition-matrix Monte Carlo simulation to study the ability of entropy scaling relationships to describe kinetic properties of the extended simple point charge water model. We examine translational and rotational diffusivities, a characteristic relaxation time for rotational motion, and a collective relaxation time stemming from analysis of the coherent intermediate scattering function. We consider both the thermodynamic excess entropy and the contribution to the two-body excess entropy related to center-of-mass correlations as scaling variables. Calculations are performed over a broad range of conditions that span from the dense supercooled liquid regime to the critical region. We find that the thermodynamic excess entropy serves as a suitable metric for describing reduced transport properties for state conditions corresponding to temperatures above the onset of water's structurally anomalous region, defined by states points for which the excess entropy increases upon compression at constant temperature. In contrast, the aforementioned two-body contribution to the excess entropy cannot be used to quantitatively predict kinetic properties over the wide range of conditions explored here. For state points above the onset temperature of the structurally anomalous region, reduced transport property data collapse onto common curves when expressed as a function of the thermodynamic excess entropy. Below this temperature, data fall onto isochore-specific curves. Our results show a relatively strong correlation between the translational diffusivity and excess entropy and a noticeably weaker correlation between rotational mobility and excess entropy.

摘要

我们使用分子动力学和过渡矩阵蒙特卡罗模拟来研究熵标度关系描述扩展简单点电荷水模型动力学性质的能力。我们研究了平移和旋转扩散系数、旋转运动的特征弛豫时间以及源自相干中间散射函数分析的集体弛豫时间。我们将热力学过剩熵和与质心相关的两体过剩熵贡献作为标度变量。计算在从密集过冷液体区域到临界区域的广泛条件范围内进行。我们发现,热力学过剩熵可作为描述高于水的结构异常区域开始时的温度下的状态条件的输运性质的合适指标,该温度由在恒温下压缩时过剩熵增加的状态点定义。相比之下,上述两体过剩熵贡献不能用于定量预测这里探索的广泛条件下的动力学性质。对于结构异常区域开始温度以上的状态点,当表示为热力学过剩熵的函数时,降低的输运性质数据会合并到共同的曲线上。在该温度以下,数据落在等压特定曲线上。我们的结果表明,平移扩散系数与过剩熵之间存在较强的相关性,而旋转迁移率与过剩熵之间的相关性较弱。

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